Olympus mons- on the moon- lacks water which makes it a better shield volcano. so these lack water.
900
to love
In Anglo-Saxon times, the cost of a shield could vary significantly based on its materials and craftsmanship. A basic wooden shield might cost around 1 to 2 shillings, while more elaborate shields made of metal or with intricate designs could cost several shillings, potentially up to 10 or more. The price also depended on the region and the wealth of the buyer, as well as the availability of resources.
Being dry means free of any liquids. Since water is a liquid and sand is a solid, sand is actually much drier than water.
The problem was that there was too much water so obviously it flooded.
Yes. Mount Kilauea is a shield volcano. If you look at Mt. Kilauea at an angle, it will look like a big cone.
A shield volcano is a type of volcano with broad, gently sloping sides that resemble a shield. They are typically much larger in area and have lower height compared to stratovolcanoes. Shield volcanoes can cover hundreds to thousands of square kilometers.
Both cinder cone and shield volcanoes are primarily composed of basaltic lava flows. However, cinder cone volcanoes are characterized by steep slopes, smaller size, and built up from pyroclastic material like ash and cinders, while shield volcanoes are much larger with gentle slopes built from numerous lava flows.
Data for a volcano can include its location, elevation, type of volcano (e.g. stratovolcano, shield volcano), history of eruptions, monitoring data (seismic activity, gas emissions), and risk assessment for surrounding communities.
The explosiveness of a volcano is determined by two factors. The obstacles in the magma's path and the type of volcano. When there is chunks of rock and hardened magma in the vent the liquid magma builds up until it sprays out at hufe ferocity. If there is little or no debris then the magma simply spews out. As for the type of volcano when the tectonic plates move apart it forms a row of GENTLE volcanoes but when they crash together the volcanoes are much more explosive.
The silica content will vary from one volcano to the next and will even vary over time for a single volcano. On average, though, composite volcanoes erupt intermediate rocks that are 52-63% silica.
A sheild cone is volcano that is sorta flat and gently sloping up.
Ocean water has a higher salinity (salt content) than fresh water does.
The percentage of water content in arrowroot stands at 63%.
The way a volcano is being formed, depends on the type of lava. Cinder cone volcanoes is made from andesitic lava. This type of lava is especially thick, and therefore is won't be able to ''run'' very far from the volcano. In this way, each time a cinder cone volcano erupts, it will create a new layer of lava, making the volcano higher and higher each time, but it will not increase its base area very much. It's different with shield volcanoes. They are made from another kind of lava which will advance very far from it's vent. Therefore the shield volcano won't often be very tall, but it can have a very large base area
the water content of an apple is 80% and the other 20% is air
About 70%